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Suspended sediment flux of river: Wavelet analysis in the Panlong basin of the Upper Red River (Honghe River), China

机译:河流悬浮泥沙通量:中国红河上游盘龙盆地的小波分析

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摘要

This paper applied wavelet analysis to examining change tendency, multi-time scale variations, periodic and abrupt change characteristics of suspended sediment flux (SSF) of the Panlong basin in the Upper Red River, China. The results indicated that the SSF had increased from 1951 to 1997, but declined since 1998. The variations of the SSF had multi-time scale characteristics and the fluctuations varied in different time periods. Three periodic time scales, 4, 7 and 22 years, were determined. The 22-year periodic time scale, which was the most obvious one among the three time scales, extended through the whole research period, whereas the 4- and 7-year time scales were obvious only in certain time periods. There were 27 times of abrupt changes across the 4-year time scale, 16 times across the 7-year time scale and 5 times across the 22-year time scale, respectively. On the basis of social statistical and climate data analysis, we concluded that the human activities were the main reason that led to the changing tendency of the SSF, but the characteristics of the multi-time scale, periodic and abrupt change were mainly influenced by climate variations.
机译:本文运用小波分析方法研究了红河上游盘龙盆地悬浮泥沙通量的变化趋势,多次尺度变化,周期性和突变特征。结果表明,SSF从1951年到1997年有所增加,但自1998年以来一直在下降。SSF的变化具有多时间尺度特征,并且波动在不同时间段变化。确定了三个周期性的时间尺度,分别是4、7和22年。 22年周期时标是三个时标中最明显的一个,在整个研究期间都得到了扩展,而4年和7年时标仅在某些时间段才很明显。在4年时间尺度上发生了27次突变,在7年时间尺度上发生了16次突变,而在22年时间尺度上发生了5次突变。在社会统计和气候数据分析的基础上,我们得出结论,人类活动是导致SSF变化趋势的主要原因,但多时标,周期性和突变性的特征主要受到气候的影响。变化。

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